Written in EnglishRead online
|Statement||J.G. Cogley ... [et. al.]|
|Series||NHRI science report -- no. 6., NHRI science report -- no. 6..|
|The Physical Object|
|Pagination||xii, 168 p. :|
|Number of Pages||168|
Download Mass balance of Axel Heiberg Island glaciers, 1960-1991
Mass balance of Axel Heiberg Island glaciers, – a reassessment and discussion. Saskatoon, Sask, Environment Canada. National Hydrology Research by: Get this from a library.
Mass balance of Axel Heiberg Island glaciers a reassessment and discussion. [J Graham Cogley; National Hydrology Research Institute (Canada);]. Buy Mass Balance of Axel Heiberg Island Glaciers a Reassessment and Discussion (NHRI Science Report No 6) by J G.
Cogley (ISBN: ) from Amazon's Book Store. Everyday low prices and free delivery on eligible : J G. Cogley. Mass balance of Axel Heiberg Island glaciers a reassessment and discussion / J.G. Cogley [et al.].
GB N7 M38 A study in glacier inventory: the ice masses of Axel Heiberg Island, Canadian Arctic archipelago / C. Ommanney. White Glacier is a valley glacier occupying km 2 in the Expedition Fiord area of Axel Heiberg Island, Nunavut, Canada (longitude °50', latitude 79°30'). It extends in elevation from 56 m to m above sea level, a range which, as noted by Dyurgerov (), is exceeded only by Devon Ice Cap in the world list of glaciers with measured mass balance.
Mass Balance of Axel Heiberg Island Glaciers. – Cogley, J.G., Adams, W.P., Ecclestone, M.A., Jung-Rothenhäusler, F., Ommanney, C.S.L., (). Try the new Google Books.
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Baby Glacier is a niche glacier occupying km 2 in the Expedition Fiord area of Axel Heiberg Island, Nunavut, Canada (longitude °58', latitude 79°26'). It lies some 8 km west of the terminus of White Glacier in the same drainage basin as Crusoe Glacier, and extends in.
The negative mass balance of most Arctic glaciers may be a response to a step-like warming in the early twentieth century at the termination of the cold Little Ice Age. Arctic ice masses outside Greenland are at present contributing about mm yr −1 to global sea-level rise.
The glacier mass balance provides information about the amount of water stored or released by a glacier within a given time period (Cogley et al., ).The glacier mass budget is characteristically evaluated over one hydrological year (October 1–September 30) and is reported as water equivalent per unit area per year (m a −1).Mass balance b (m a −1) at one point on the glacier surface.
The Axel Heiberg Glacier in Antarctica is a valley glacier, 30 nmi (35 mi) long, descending from the high elevations of the Antarctic Plateau into the Ross Ice Shelf (nearly at sea level) between the Herbert Range and Mount Don Pedro Christophersen in the Queen Maud Mountains.
This huge glacier was discovered in November by the Norwegian polar explorer Roald Amundsen, and named by him. M.A. Ecclestone's 14 research works with citations and reads, including: Comparison of geodetic and glaciological mass budgets for White Glacier, Axel Heiberg Island, Canada.
Axel Heiberg Island: | | Axel Heiberg | | | ||| | World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most.
Michael (Mike) Hambrey graduated from Manchester University with a degree in Geography and Geology in and a PhD in Glaciology in He then spent three years as a Post-Doctoral Research Associate (PDRA) at Mass balance of Axel Heiberg Island glaciers Swiss Federal Institute of Technology in Zurich, and a further 14 years as a Research Associate in the Department of Earth Sciences and the Scott Polar Research Institute at the.
Mass Balance of Axel Heiberg Island Glaciers A Reassessment and Discussion by J. Cogley, W. Adams, M. Ecclestone, E Jung-Rothenhaiuser, and C. Ommanney; Glacier Mass Balance Bulletin. Bulletin No.
3 () edited by Wilfried. - Changes in velocity of White Glacier, Axel Heiberg Island, Canada, over the past 50 years Luke Copland, S. Thomson - Glacier Velocity Variation and Surge Type Glaciers on Manson Iceﬁeld, Southeast Ellesmere Island - Danielle Hallé, L: Copland - Coffee break Methods Convener: Francisco Navarro.
UNESCO/IASH,Combined heat, ice and water balances at selected glacier basins, a guide for compilation and assemblage of data for glacier mass balance measurements: UNESCO/IASH Tech. Papers in Hydrology, no. 5,20 p. Baby Glacier, Axel Heiberg Island, N.W.T., Canada is a small ( km2), high-latitude (79°N), high-altitude (– m) glacier with a mass balance record extending from –60 to the present.
The Canada Glacier (77°37′S, °55′E) is located in the McMurdo Dry Valleys of Antarctica. The White Glacier (79°27′N, 90°40′W) is located on Axel Heiberg Island, Nunavut Territory, Canada.
These glaciers are at similar, yet antipodal latitudes, are roughly the same size and endure approximately the same mean annual temperature. Proceedings of the workshop at Riederalp, Switzerland, Septemberorganized by the Temporary Technical Secretariat for the World Glacier Inventory.
Main topics discussed were: techniques of glacier inventory data compilation; specific inventory difficulties with Greenland and Antarctica, rock glaciers, surging glaciers, firn and equilibrium lines, glacier identification and.
Fritz Müller engaged in geodetic survey work, White Glacier, Axel Heiberg Island, Canada (Peter Adams). mass balance of a glacier is a measure of the change in mass of the glacier, or part of it, over a period measurements are made on fewer than glaciers.
Mass-balance information is essential for defining. Analysis of the SMB record (figure 2) reveals that these glaciers were in balance between and with an ice discharge of ± Gt yr −1 (figure 2) versus a SMB of ± Gt yr −1.
Afterthe mass balance decreased from + ± Gt yr −1 (i.e. a mass. TTL Cook Book, A electronic book that has everything to do with Mass balance of Axel Heiberg Island glaciers, a reassesssment and discussion Measurement, Glaciers -- Northwest Territories -- Axel Heiberg Island, Mass budget Books to Borrow.
7 Canadian native law cases: with comprehensive subject index. Ommanney’s () detailed inventory of Axel Heiberg Island glaciers, based on photography from –59, has been revisited, converted into digital format and compared to glacier extents mapped from – satellite imagery.
Our results show that the island-wide ice coverage decreased by km2 in the 42year period, a loss of. Small glaciers are highly sensitive to recent climate warming yet notably understudied, particularly at individual basin scales.
As part of this project, Braden is conducting fieldwork to study the long-term mass losses and future fate of Baby Glacier on Axel Heiberg Island, Nunavut.
The four annual surface mass balance records, spanning the 41 yr from toare not well correlated with each other (r = –), but they nevertheless display strong underlying 1 of these records has an eigenvalue of and accounts for 53% of the variance across the four time series ().The loadings of the four mass balance time series on PC1 are similar in.
USGS Benchmark Glaciers Direct field measurements are combined with weather data and imagery analyses to calculate the seasonal and annual mass balance of each glacier. This data release includes seasonal and annual glacier-wide mass balance, and the input point measurements and elevation data used for these calculations.
Infobox Islands name = Axel Heiberg image caption = Closeup of Axel Heiberg Island image size = locator. Axel Heiberg Island (Inuktitut: ᐅᒥᖕᒪᑦ ᓄᓈᑦ, Umingmat Nunaat) is an island in the Qikiqtaaluk Region, Nunavut, d in the Arctic Ocean, it is the 32nd largest island in the world and Canada's seventh largest ing to Statistics Canada, it has an area of 43, km 2 (16, sq mi).
It is named after Axel Heiberg. One of the larger members of the Canadian. EXPEDITION FIORD, AXEL HEIBERG ISLAND Measurements of glaciers around Expedition Fiord, western Axel Heiberg Island, Nunavut (Fig. 1), began in Some of those measurement series, including mass-balance measurements on Baby and White glaciers, now extend over 50 years.
Both glaciers have experienced nega-tive mass balances since the s. Figure 1 Benchmark glacier mass balance monitoring and assessment sites for western Canada, Alaska and the coterminous USA.
W.P., Ecclestone, M.A., Jung-Rothenhausler, F., and Ommanney, C.S.L.,Mass balance of Axel Heiberg Island glaciers A reassessment and discussion: National Hydrology Research Institute Science.
In addition the journal publishes opinion pieces, book reviews and in memoria. AAAR is associated with the Institute of Arctic and Alpine Research (INSTAAR) the oldest active research institute at the University of Colorado Boulder.
Coverage: (Vol. 1, No. 1 - Vol. 30, No. On neighboring Axel Heiberg Island, glaciologists Miles Ecclestone of Trent University and Luke Copland of the University of Ottawa are measuring how much mass the glaciers. Basantes-Serrano, R. et al. Slight mass loss revealed by reanalyzing glacier mass-balance observations on Glaciar Antisana 15α (inner tropics) during the – period.
Glaciol. 62. Annual net balance of North Cascade glaciers, Mauri S. Pelto. Measurement of ice-sheet topography using satellite-radar interferometry Ian Joughin, Dale Winebrenner, Mark Fahnestock, Ron Kwok and William Krabill. The thermal regime of sub-polar glaciers mapped by multi-frequency radio-echo sounding.
Mass Balance of Glaciers ; Ice Shelf Dynamics; Publications. Axel Heiberg; Axel Heiberg ; McMurdo Dry Valleys ; McMurdo Dry Valleys ; (Chinn ). Most of the glacier-covered area is in the South Island with approximately the same areas on the west and east coasts but a greater volume on the east coast (Figure 1).
Global Energy Balance Archive, GEBA: World Climate Program--Water, project A7 by Atsumu Ohmura (Book) 23 editions published.
Among the most dramatic evidence that Earth's climate is warming is the dwindling and disappearance of mountain glaciers around the world. Based on preliminary data, is likely to be the 30 th year in a row of mass loss of mountain glaciers worldwide.
According to the State of the Climate inThe cumulative mass balance from to is − m, the equivalent of cutting a m. 1 Introduction and Study Area. The Queen Elizabeth Islands (QEI; Devon, Ellesmere, and Axel Heiberg Islands; Figure 1 inset) contain ~, km 2 of glacier ice, which represents 25% of Arctic glacier ice outside the Greenland Ice Sheet [Arendt et al., ].Long‐term surface mass balance records from this region indicate that prior to the late s the ice masses were largely in balance.
Discussion of “Glacier velocities and dynamic discharge from the ice masses of Baffin Island and Bylot Island, Nunavut, Canada” 1.
Simon L. Ommanney. 56. four glaciers between the Liv and the Amundsen Glaciers, which flow from the Polar Plateau. But these four glaciers, of which the Axel Heiberg is '!'This article is to be published in the Yearbook (Arbok ) of the Norsk Polarinstitutt, Oslo, early in N Z.
]. c-»s. 5: in the extent and volume of glaciers in the region since the end of the Little Ice Age and the contribu-tion of glacier change to global sea level. REGIONAL CONTEXT Geology and physiography The larger islands in the eastern Canadian Arctic (Ellesmere Island, Devon Island, Axel Heiberg Island, Bylot Island, and Baﬃn Island) are rugged.
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